The 1902 Peléean deposits in the Fort Cemetery of St. Pierre, Martinique: a model for the accumulation of turbulent nuées ardentes
- 8 April 2003
- journal article
- Published by Elsevier
- Vol. 38 (1-2) , 113-129
- https://doi.org/10.1016/0377-0273(89)90033-4
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Ignimbrite types and ignimbrite problemsPublished by Elsevier ,2003
- Mt. Pelée, martinique: may 8 and 20, 1902, pyroclastic flows and surgesPublished by Elsevier ,2003
- Characteristics of dune-bedded pyroclastic surge bedsetsJournal of Volcanology and Geothermal Research, 1984
- Comments and Reply on “Mount St. Helens 1980 and Mount Pelée 1902—Flow or surge?”Geology, 1984
- Flow-head deposits in ash turbiditesGeology, 1983
- Fines-depleted ignimbrite in New Zealand — The product of a turbulent pyroclastic flowGeology, 1980
- Destruction of St. Pierre, Martinique, by ash-cloud surges, May 8 and 20, 1902Geology, 1980
- The anatomy and interpretation of an Archean volcaniclastic sequence, Noranda region, QuebecCanadian Journal of Earth Sciences, 1978
- Grain size variations in ignimbrites and implications for the transport of pyroclastic flowsSedimentology, 1976
- EXPERIMENTS ON DENSITY AND TURBIDITY CURRENTS: III. DEPOSITION OF SEDIMENTCanadian Journal of Earth Sciences, 1967